『Abstract
Denitrification is an important process of nitrogen cycling in
river ecosystems as it can regulate nitrogen availability, and
therefore primary production, controlling the degree of eutrophication.
The strength of denitrification within a river network can alternate
very rapidly in space and time and is essentially driven by the
interactions between surface water, river geomorphology and microbial
process rates. In this study, benthic denitrification was quantified
over an entire drainage network by linking a deterministic sediment
module [Thouvenot M., Billen G., Garnier J., 2007. Modelling nutrient
exchange at the sediment-water interface of river systems. J.
Hydrol. 341(1-2), 55-78] to a hydrological/biogeochemical model
(Riverstrahler). The benthic module included the calculation of
nutrient exchanges across the sediment-water interface as a result
of the sedimentation flux of organic material provided by Riverstrahler.
Along the Seine, the coupled model was able to reproduce nutrients
concentrations in the water and the impact of pollution from point
sources in terms of fluxes across the sediment-water interface.
Over the entire drainage network of the Seine river system the
model simulated the observed increase of organic matter content
in the sediment with stream order and its subsequent increase
of oxygen and nutrients fluxes at the sediment-water interface.
Moreover, due to the high variability of denitrification in space
and time, Riverstrahler is a better tool to approximate denitrification
over an entire year and drainage network than a calculation based
on sparse direct measurements of benthic denitrification. Finally,
the nitrogen budgets of two different hydrological years (wet
and dry) showed that although for both years riparian denitrification
was more important than benthic denitrification, the latter could
not be neglected during dry years as it contributed to up to 10%
of the losses from river inputs.
Keywords: Denitrification; Sediment; Model; River network』
Introduction
Model description
Riverstrahler
Riparian denitrification
Water column denitrification
Benthic module
Link between the RIVERSTAHLER and the benthic module
The Seine case study
Non-point sources of nitrogen
Point sources of nitrogen
Results
Consistency of the stand alone benthic module
Combined model
Hydrology
Benthic fluxes over longitudinal profiles
Benthic fluxes by stream order
Discussion
Conclusion
Acknowledgements
References